Abstract
The cooling history of rocks is manifested in the microstructures of their minerals, which are most conveniently observed by TEM. To help in their interpretation, X-ray diffraction of heated single crystals is applied.
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© 1991 Springer-Verlag Berlin Heidelberg
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Feuer, H., Schröpfer, L., Fuess, H. (1991). Microstructures and Thermal Behaviour of Igneous Pyroxenes. In: Voll, G., Töpel, J., Pattison, D.R.M., Seifert, F. (eds) Equilibrium and Kinetics in Contact Metamorphism. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-76145-4_6
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DOI: https://doi.org/10.1007/978-3-642-76145-4_6
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-76147-8
Online ISBN: 978-3-642-76145-4
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